Atmospheric Boundary Layers Nature, Theory, and Application to Environmental Modelling and Security /
Most of practically-used turbulence closure models are based on the concept of downgra- ent transport. Accordingly the models express turbulent uxes of momentum and scalars as products of the mean gradient of the transported property and the corresponding turbulent transport coef cient (eddy viscosi...
Clasificación: | Libro Electrónico |
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Autor Corporativo: | |
Otros Autores: | , |
Formato: | Electrónico eBook |
Idioma: | Inglés |
Publicado: |
New York, NY :
Springer New York : Imprint: Springer,
2007.
|
Edición: | 1st ed. 2007. |
Temas: | |
Acceso en línea: | Texto Completo |
Tabla de Contenidos:
- Atmospheric boundary layers: nature, theory and applications to environmental modelling and security
- Some modern features of boundary-layer meteorology: a birthday tribute for Sergej Zilitinkevich
- Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes
- Similarity theory and calculation of turbulent fluxes at the surface for the stably stratified atmospheric boundary layer
- Application of a large-eddy simulation database to optimisation of first-order closures for neutral and stably stratified boundary layers
- The effect of mountainous topography on moisture exchange between the "surface" and the free atmosphere
- The influence of nonstationarity on the turbulent flux-gradient relationship for stable stratification
- Chemical perturbations in the planetary boundary layer and their relevance for chemistry transport modelling
- Theoretical considerations of meandering winds in simplified conditions
- Aerodynamic roughness of the sea surface at high winds
- Modelling dust distributions in the atmospheric boundary layer on Mars
- On the turbulent Prandtl number in the stable atmospheric boundary layer
- Micrometeorological observations of a microburst in southern Finland
- Role of land-surface temperature feedback on model performance for the stable boundary layer
- Katabatic flow with Coriolis effect and gradually varying eddy diffusivity
- Parameterisation of the planetary boundary layer for diagnostic wind models.